Karst resilience refers to the capacity of a karst system to absorb and recover from disturbances, such as changes in climate, land use, or pollution.

Human activities are not considered a key component of karst resilience, as they can often be a source of disturbance or degradation.

Dissolution is the primary driver of karst landscape evolution, as it is the process by which soluble rocks, such as limestone and dolomite, are dissolved by water.

Uvalas are not a common type of karst landform, as they are typically associated with non-karst environments.

Exfiltration is the term used to describe the process by which water flows out of a karst aquifer, typically through springs or seeps.

Urbanization is not typically considered a potential threat to karst environments, as it is often associated with non-karst areas.

Recharge is the term used to describe the process by which a karst aquifer is replenished with water, typically through infiltration or percolation.

Glacial caves are not a common type of karst cave, as they are typically associated with non-karst environments.

Karst formation is the term used to describe the process by which a karst landscape is created, typically through the dissolution of soluble rocks.

Thermal springs are not a common type of karst spring, as they are typically associated with non-karst environments.

Exfiltration is the term used to describe the process by which a karst aquifer is depleted, typically through springs or seeps.

Perched poljes are not a common type of karst polje, as they are typically associated with non-karst environments.

Karst denudation is the term used to describe the process by which a karst landscape is eroded, typically through the action of water, wind, and ice.

Glacial sinkholes are not a common type of karst sinkhole, as they are typically associated with non-karst environments.

Karst rejuvenation is the term used to describe the process by which a karst landscape is rejuvenated, typically through the action of tectonic uplift or climate change.